THE MINERALOID LECHATELIERITE

Lechatelierite is considered a mineraloid because it lacks a crystal structure.
It is actually made of fused silica; SiO2.Quartz is also made of silica, but it has a crystalline structure.
Basically lechatelierite is glass! However, it differs from regular glass by virtue of its natural origins.
Lechatelierite is also not the same as
obsidian.
Although obsidian is considered a natural glass it is not pure
SiO2.
And although lechatelierite is sometimes formed as a result of meteorite impacts like
tektites, they are not the same.
Unless the tektites are very pure silica as in the case of a variety called Libyan Glass (see above).
To sum all of this up, lechatelierite is natural, pure or nearly pure, silica glass.

Lechatelierite has three different origins: Meteorite impacts, volcanism and lightning strikes.
The meteorite impacts simply fused quartz grains in the impacted rocks with the incredible pressures that they generate.
The volcanism origin is the same as for obsidian, where molten rock cools too quickly for a crystalline structure to form.
But as was explained before, obsidian is generally a mix of several chemistries besides SiO2.
The lightning strike origin is perhaps the most interesting.

When lightning strikes the earth in sandy areas such as deserts or sandy beaches, the intense heat and energy of the bolt will fuse the sand grains in a milli-second.
A branching, hollow, glassy tube is sometimes the result.
These "fossil" lightning strikes are composed of lechatelierite and occassionally fused biotite or other minerals.
They are referred to as fulgarites and are certainly a natural history oddity.
Fulgarites have been found that were several feet in length, although most are a few inches long by a half inch thick.

PHYSICAL CHARACTERISTICS:

Color is white, colorless or pale yellow; some fulgarites can be pale brown, gray or black.

Luster is vitreous.

Transparency: Specimens are translucent.

Crystal System: Does not apply because lechatelierite is
amorphous.

Habits include disseminated grains in volcanic rocks and shatter zones of meteorite impacts and as tube shaped fulgarites (see above).